Comments |
The assigned preferred vertical slip rate is based on reconnaissance studies by Lundstrom (1986) and Mathieson (1983); both report a slip rate of 0.4 mm/yr for the late Pleistocene. More recent studies by Ruleman (2002) suggest a range of similar slip rates that average 0.4 mm/yr. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Mathieson, E.L., 1983, Late Quaternary activity of the Madison Range fault along its 1959 rupture trace, Madison County, Montana: Stanford, California, Stanford University, unpublished M.S. thesis, 169 p., 4 pls. Lundstrom, S.C., 1986, Soil stratigraphy and scarp morphology studies applied to the Quaternary geology of the southern Madison Valley, Montana: Arcata, California, Humboldt State University, unpublished M.S. thesis, 53 p., 1 pl., scale 1:24,000. Ruleman, C.A., III, 2002, Quaternary tectonic activity within the northern arm of the Yellowstone tectonic parabola and associated seismic hazards, southwest Montana: Bozeman, Montana State University, unpublished M.S. thesis, 158 p. Lund, W.R., ed., 2006, Basin and Range Province Earthquake Working Group seismic-hazard recommendations to the U.S. Geological Survey National Seismic Hazard Mapping Program: Utah Geological Survey Open-File Report 477, 23 p, ugspub.nr.utah.gov/publications/open_file_reports/OFR-477.pdf.
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